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2006 | 27 | 3 |

Tytuł artykułu

A meteorological study of the ablation process on Hans Glacier, SW Spitsbergen

Warianty tytułu

Języki publikacji

EN

Abstrakty

EN
The ablation of glaciers is an important factor in energy exchange between the atmosphere and land ice masses. The dynamics of ablation closely reflects climate changes and is important for the estimation of the outflow of meltwater, which, having penetrated a glacier to bedrock, stimulates its velocity by increasing basal sliding. More detailed studies using automatic weather stations (AWS) and the calculation of the energy budget are rarely conducted on small glaciers. The mass balance of the Hans Glacier has been monitored since 1989. Its intensified monitoring using AWS began in 2003. The results show that ablation depends more evidently on the daily mean and maximum air temperature and wind speed than on total and net radiation. Ablation, both that controlled by sonic height ranger and that measured manually on stakes, was compared with the values calculated on the basis of energy flux formulas applied by Oerlemans (2000). The statistical results allowed us to construct empirical equations, which in turn enabled us to compute the course and total ablation during the summer seasons. It can be described on the basis of two primary meteorological elements (air temperature and wind speed), as recorded in the station representing the regional area (Hornsund) or measured in situ on the glacier. Standard measurements of ablation from the years 1989-2004 were used to verify empirical model. The computed mean value of summer ablation for 1989-2004 was calculated at 1.35 m, differing from real measurements by only 10% (with SD = 0.18). The results obtained illustrate that an empirical equation can be applied in time series analyses. A regional ablation model enables us to investigate the mass-balance history of glaciers on the basis of meteorological data.

Wydawca

-

Rocznik

Tom

27

Numer

3

Opis fizyczny

p.243-258,fig.,ref.

Twórcy

autor
  • Wroclaw University, Kosiby 6/8, 51-670 Wroclaw, Poland
autor
autor

Bibliografia

  • Baranowski S. 1977. Subpolarne lodowceSpitsbergenunatleklimatu tegoregionu.Acta Universi- tatis Wratislaviensis 393: 157 pp (in Polish).
  • Braithwaite R.J. 1995. Positive degree-day factors for ablation on the Greenland ice sheet studied by energy-balance modeling. Journal of Glaciology 41 (137): 153-160.
  • Braithwaite R.J. and Olesen O.B. 1989. Calculation of glacier ablation from air temperature, West Greenland. In: J. Oerlemans (ed.) Glacier Fluctuations and Climatic Change. Kluwer Academic Publishers, Dordrecht: 219-233.
  • Eagleson P.S. 1978. Hydrologia dynamiczna. PWN, Warszawa: 501 pp. (in Polish).
  • Hock R. 1998. Modeling of glacier melt and discharge. Züricher Geographische Schriften 70: 1-126.
  • Hock R. 1999. A distributed temperature-index ice- and snowmelt model including potential direct solar radiation. Journal of Glaciology 45 (149): 101-111.
  • Jania J. 1997. Glacjologia. PWN, Warszawa: 360 pp. (in Polish).
  • Jania J., Mochnacki D. and Gądek B. 1996. The thermal structure of Hansbreen, a tidewater glacier in southern Spitsbergen, Svalbard. Polar Research 15 (1): 53-66.
  • Johannesson T., Sigurdsson O., Laumann T. and Kennett M. 1995. Degree-day glacier mass-balance modeling with applications to glaciers in Iceland, Norway and Greenland. Journal of Glaciology 41 (138): 345-358.
  • Krenke A.N. and Khodakov V.G. 1966. O svyasi povercknostnogo tayaniya lednikov s temperaturoy vozdukha (On the relationship between melt of glaciers and air temperature). Materialy Glyatsiologicheskikh Issledovaniy 12: 153-163 (in Russian).
  • Laumann T. and Reeh N. 1993. Sensitivity to climate change of the mass balance of glaciers in Southern Norway. Journal of Glaciology 39 (133): 656-665.
  • Moore J.C., Palli A., Ludwig F., Blatter H., Jania J., Gądek B., Głowacki P., Mochnacki D. and Isaksson E. 1999. High-resolution hydrothermal structure of Hansbreen, Spitsbergen, mapped by ground-penetrating radar. Journal of Glaciology 45 (151): 524-532.
  • Oerlemans J. 1988. Simulation of historic glacier variations with a simple climate-glacier model. Journal of Glaciology 34 (118): 333-341.
  • Oerlemans J. 2000. Analysis of a 3 year meteorological record from the ablation zone of Morteratsch- gletscher, Switzerland: energy and mass balance. Journal of Glaciology 46 (155): 571-579.
  • Röthlisberger H. and Lang H. 1987. Glacial Hydrology In: A.M. Gurnell and M.J. Clark (eds) Glacio-fluvial sediment transfer. An alpine perspective. J. Wiley and Sons Ltd., London: 207-284.

Typ dokumentu

Bibliografia

Identyfikatory

Identyfikator YADDA

bwmeta1.element.agro-article-8bb6b459-6b7b-4d5c-9177-6e108bd12a27
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